Figure F35. Magnetic susceptibility data, Site U1332. A. Magnetic susceptibility data from Cores 320-U1332A-7H through 9H, 320-U1332B-7H through 9H, and 320-U1332C-7H through 9H. Note similar pattern in Cores 8H and 9H of each hole. B. Correlation of magnetic susceptibility data from Cores 320-U1332B-7H through 9H and 320-U1332C-7H through 9H to Cores 320-U1332A-7H through 9H, illustrating the actual sequence of sediment at U1332. Note gaps between Cores 320-U1332A-7H through 9H have been expanded artificially for straightforward correlation. C. Correlation of magnetic susceptibility data from Cores 320-U1332A-7H through 9H, 320-U1332B-7H through 9H, and 320-U1332C-7H through 9H to ODP Site 1220. The strong similarity between observed patterns allows for detailed correlation between all three holes and confirms duplication of sediments and recovery of a complete stratigraphic record. The sharp contact observed in Section 320-U1332C-9H-2 (core image) marks the base of the duplicated interval.
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